吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (2): 355-366.doi: 10.13278/j.cnki.jjuese.20200037
• 地质与资源 • 上一篇
刘峻桥1,2,3, 吕延防1, 付广1, 胡欣蕾1, 史集建1, 孙同文2,3
Liu Junqiao1,2,3, Lü Yanfang1, Fu Guang1, Hu Xinlei1, Shi Jijian1, Sun Tongwen2,3
摘要: 断层圈闭是斜坡区重要的构造圈闭类型,为了识别斜坡区断层圈闭发育部位及其形成时期,基于断层生长机制,分析斜坡区顺向断层圈闭和反向断层圈闭形成演化过程。结果表明:顺向断层圈闭形成于断层"硬连接"阶段,发育在断层下降盘分段生长部位;反向断层圈闭形成于断层开始活动时期,发育在断层上升盘位移最大部位。在此基础上,充分利用详细三维地震资料,结合断距-距离曲线、相干体切片、断层分段生长时期定量表征以及断距回剥等技术,建立了斜坡区断层圈闭发育部位及形成时期的识别方法,并将该方法应用于冀中坳陷文安斜坡典型断层圈闭发育部位及形成时期的识别,研究结果与实际油气分布吻合关系较好。
中图分类号:
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